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Influence of Global Climate Changes in Past Centuries on the Chemical Composition of Bottom Sediments in the Chukchi Sea


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Abstract

The sedimentary cores from the southern and northern parts of the Chukchi Sea illustrate the influence of climate and environmental conditions on the chemical composition of bottom sediments accumulated at present and in the recent 500 years. The low concentration of biogenic (Ca, Br, Sr) and some redox-sensitive (Fe, Mn, Zn) elements is typical of the recent sediments accumulated in the areas with permanent ice cover and of the sediments accumulated during cold periods (Little Ice Age and especially the Maunder Minimum). The possibility is revealed of identifying cyclic changes in environmental conditions including sea ice extent in the concrete Arctic areas. This may be used to detail the regional forecast of future changes.

About the authors

A. S. Astakhov

Il’ichev Pacific Oceanological Institute, Far Eastern Branch

Author for correspondence.
Email: astakhov@poi.dvo.ru
Russian Federation, ul. Baltiiskaya 43, Vladivostok, 690041

E. G. Vologina

Institute of the Earth’s Crust, Siberian Branch

Email: astakhov@poi.dvo.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033

A. V. Dar’in

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: astakhov@poi.dvo.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090

I. A. Kalugin

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: astakhov@poi.dvo.ru
Russian Federation, pr. Akademika Koptyuga 3, Novosibirsk, 630090

V. V. Plotnikov

Il’ichev Pacific Oceanological Institute, Far Eastern Branch

Email: astakhov@poi.dvo.ru
Russian Federation, ul. Baltiiskaya 43, Vladivostok, 690041

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